摘要
在内蒙古东部的大兴安岭中南段地区,具有工业价值的多数大中型银多金属矿床均产于二叠系中。笔者在敖脑达坝铜-银-锡矿床开展研究时,对该矿区西部出露的凝灰质板岩取样并开展了LA-MC-ICP-MS测年工作,获得的锆石U-Pb年龄为(302.6±1.9)Ma,MSWD=2.0,表明凝灰质板岩的原岩形成年代为晚石炭世,而不是前人认为的二叠纪。这一新发现可能对重新认识该区的区域地质演化具有重要意义。
Most economically important medium-to large-sized Ag-polymetallic deposits occurring in south-central part of the Da Hinggan Mountains in east Inner Mongolia are hosted by Permian strata.The LA-MC-ICP-MS dating of zircons from tuffaceous slate outcropped in the western part of the Aonaodaba Cu-Ag-Sn deposit yielded an U-Pb age of（302.6±1.9） Ma with MSWD being 2.0,which indicates that the original rock of the tuffaceous slate was formed in late Carboniferous instead of in Permian considered by previous researchers.This new discovery is of great significance for re-understanding the regional geological evolution.
出处
《矿床地质》
CAS
CSCD
北大核心
2012年第1期161-164,共4页
Mineral Deposits
基金
国家重点自然科学基金项目(41030421)
全国危机矿山项目(20089948)
地质大调查项目(1212010911029)联合资助
